(i.e., the zonal average of vT), where x2 - x1 = 2na cos p, where a is the Earth's radius and p latitude.

Use the figure to estimate the net northward heat flux by eddies across 45° N. Compare this with the requirement (from the Earth's radiation budget and Fig. 8.13 that the net (atmosphere and ocean) heat transport must be about 5 x 1015 W.

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